Rain Attenuation in the Microwave-to-Terahertz Waveband

S. Ishii, M. Kinugawa, S. Wakiyama, S. Sayama, T. Kamei
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引用次数: 16

Abstract

In recent years, there has been increased interest in the terahertz waveband for application to ultra-high-speed wireless communications and remote sensing systems. However, atmospheric propagation at these wavelengths has a significant effect on the operational stability of systems using the terahertz waveband, so elucidating the effects of rain on propagation is a topic of high interest. We demonstrate various methods for calculating attenuation due to rain and evaluate these methods through comparison with calculated and experimental values. We find that in the 90 - 225 GHz microwave band, values calculated according to Mie scattering theory using the Best and P-S sleet raindrop size distributions best agree with experimental values. At 313 and 355 GHz terahertz-waveband frequencies, values calculated according to Mie scattering theory using the Weibull distribution and a prediction model following ITU-R recommendations best agree with experimental values. We furthermore find that attenuation due to rain increases in proportion to frequency for microwave-band frequencies below approximately 50 GHz, but that there is a peak at around 100 GHz, above which the degree of attenuation remains steady or decreases. Rain-induced attenuation increases in proportion to the rainfall intensity.
微波到太赫兹波段的雨衰减
近年来,人们对太赫兹波段在超高速无线通信和遥感系统中的应用越来越感兴趣。然而,这些波长的大气传播对使用太赫兹波段的系统的运行稳定性有显著影响,因此阐明雨对传播的影响是一个高度感兴趣的话题。我们展示了各种计算降雨衰减的方法,并通过与计算值和实验值的比较来评价这些方法。我们发现,在90 ~ 225 GHz微波波段,用Best和P-S雨夹雪雨滴尺寸分布计算的Mie散射理论值与实验值最吻合。在313 GHz和355ghz太赫兹频段,根据米氏散射理论、使用威布尔分布和遵循ITU-R建议的预测模型计算的值与实验值最吻合。我们进一步发现,在大约50 GHz以下的微波频段,由于降雨导致的衰减与频率成比例增加,但在100 GHz左右有一个峰值,在此之上衰减程度保持稳定或下降。降雨引起的衰减与降雨强度成正比。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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